if the treaty of versailles war fair, the second world war would war would not have occurred."how do you justify this statement?​

The correct answer to this open question is the following.

Although there are no options attached we can say the following.

The quote is "if the Treaty of Versailles war fair, the Second World War would not have occurred."

I can justify this statement? in the following way.

The victorious allies in World War I forced Germany to pay for war reparations. Yes, France and Great Britain did not really want a peace treaty. They wanted retribution and forced Germany to pay for all the destruction created during the war.

Germany was especially opposed to Article 231 of the Treaty of Versailles because it held Germany (and Austria) responsible for the war and required reparations. Germany also was forced to disarm its military.

In the end, this also resulted in a substantial loss of territory for Germany. All of these decisions and actions created so much pain and resentment in Germany. They helped set the stage for European conflict that would eventually result in World War II.

the minoans were group of people living in the greek islands of crete in the mediterranean sea during the bronze age

the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)